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高压核磁共振显示,脱辅基肌红蛋白是一种从天然态到未折叠态的平衡混合物。

High pressure NMR reveals that apomyoglobin is an equilibrium mixture from the native to the unfolded.

作者信息

Kitahara Ryo, Yamada Hiroaki, Akasaka Kazuyuki, Wright Peter E

机构信息

Department of Molecular Science, Graduate School of Science and Technology, Kobe University, 1-1 Rokkodai-cho, Nada-ku, Kobe 657-8501, Japan.

出版信息

J Mol Biol. 2002 Jul 5;320(2):311-9. doi: 10.1016/S0022-2836(02)00449-7.

DOI:10.1016/S0022-2836(02)00449-7
PMID:12079388
Abstract

Pressure-induced reversible conformational changes of sperm whale apomyoglobin have been studied between 30 bar and 3000 bar on individual residue basis by utilizing 1H/15N hetero nuclear single-quantum coherence two-dimensional NMR spectroscopy at pH 6.0 and 35 degrees C. Apomyoglobin showed a series of pressure-dependent NMR spectra as a function of pressure, assignable to the native (N), intermediates (I), molten globule (MG) and unfolded (U) conformers. At 30 bar, the native fold (N) shows disorder only in the F helix. Between 500 bar and 1200 bar, a series of locally disordered conformers I are produced, in which local disorder occurs in the C helix, the CD loop, the G helix and part of the H helix. At 2000 bar, most cross-peaks exhibit severe line-broadening, suggesting the formation of a molten globule, but at 3000 bar all the cross-peaks reappear, showing that the molten globule turns into a well-hydrated, mobile unfolded conformation U. Since all the spectral changes were reversible with pressure, apomyoglobin is considered to exist as an equilibrium mixture of the N, I, MG and U conformers at all pressures. MG is situated at 2.4+/-(0.1) kcal/mol above N at 1 bar and the unfolding transition from the combined N-I state to MG is accompanied by a loss of partial molar volume by 75+/-(3) ml/mol. On the basis of these observations, we postulate a theorem that the partial molar volume of a protein decreases in parallel with the loss of its conformational order.

摘要

在pH值为6.0、温度为35摄氏度的条件下,利用1H/15N异核单量子相干二维核磁共振光谱,在30巴至3000巴的压力范围内,对抹香鲸脱辅基肌红蛋白压力诱导的可逆构象变化进行了基于单个残基的研究。脱辅基肌红蛋白显示出一系列随压力变化的压力依赖性核磁共振谱,可归因于天然构象(N)、中间体构象(I)、熔球构象(MG)和无规卷曲构象(U)。在30巴时,天然折叠构象(N)仅在F螺旋中表现出无序。在500巴至1200巴之间,产生了一系列局部无序的构象I,其中C螺旋、CD环、G螺旋和部分H螺旋出现局部无序。在2000巴时,大多数交叉峰出现严重的线宽展宽,表明形成了熔球构象,但在3000巴时所有交叉峰重新出现,表明熔球构象转变为水合良好的、可移动的无规卷曲构象U。由于所有光谱变化随压力都是可逆的,因此脱辅基肌红蛋白在所有压力下都被认为是以N、I、MG和U构象的平衡混合物形式存在。在1巴时,MG比N高2.4±(0.1)千卡/摩尔,从N-I组合态到MG的去折叠转变伴随着偏摩尔体积减少75±(3)毫升/摩尔。基于这些观察结果,我们提出一个定理:蛋白质的偏摩尔体积与其构象有序性的丧失呈平行下降。

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